福建泉州湾海岸带MIS 3阶段以来的海侵—海退过程

赵红梅; 毛欣; 刘春雷; 李亚松; 刘林敬

doi:10.12090/j.issn.1006-6616.2023046

福建泉州湾海岸带MIS 3阶段以来的海侵—海退过程

1.
中国地质科学院水文地质环境地质研究所，河北石家庄 050061

2.
中国地质科学院第四纪年代学与水文环境演变重点实验室，河北石家庄 050061

3.
福建省水循环与生态地质过程重点实验室，福建厦门 361009

基金项目: 中国地质调查局地质调查项目（DD20190303，DD20221773，DD20221929）；中国地质科学院水文地质环境地质研究所基本科研业务费项目（SK202105，SK202213）

详细信息

作者简介: 赵红梅（1981—），女，博士，高级工程师，主要从事第四纪地层与沉积环境研究。E-mail：zhmay81@126.com

通讯作者: 毛欣（1989—），男，博士，副研究员，主要从事第四纪环境演变研究。E-mail：maoxin.iheg@cnu.edu.cn

中图分类号: P534.63

收稿日期: 2023-03-31

修回日期: 2023-06-11

录用日期: 2023-07-20

刊出日期: 2023-08-28

Transgression–regression processes since the MIS 3 in the coastal zone of Quanzhou Bay, Fujian

1.
The Institute of Hydrogeology and Environmental Geology, Shijiazhuang 050061, Hebei, China

2.
Key Laboratory of Quaternary Chronology and Hydro-Environmental Evolution, China Geological Survey, Shijiazhuang 050061, Hebei, China

3.
Fujian Provincial Key Laboratory of Water Cycling and Eco-Geological Processes, Xiamen 361009, Fujian, China

Fund Project: This research is financially supported by the Geological Survey Projects of the China Geological Survey (Grants DD20190303, DD20221773 and DD20221929) and the Special Fund of Chinese Central Government for Basic Scientific Research Operations in Commonweal Research Institutes (Grants SK202105 and SK202213).

More Information

Corresponding author: MAO Xin, maoxin.iheg@cnu.edu.cn

Received Date: 31 March 2023

Revised Date: 11 June 2023

Accepted Date: 20 July 2023

Publish Date: 28 August 2023

摘要

摘要:
海岸带是海陆相互作用的敏感地带，是沿海地区研究第四纪海侵—海退过程的理想场所。基于福建泉州湾沿岸两个第四纪钻孔岩芯（DZ01、DZ02），以地层岩性和岩相组合特征为基础，利用加速器质谱碳同位素（AMS-¹⁴C）和光释光（OSL）两种测年方法建立地层年代框架，结合泉州湾现代沉积物具有指相性的地球化学元素含量统计分析结果，运用地球化学元素比值、有孔虫和介形类环境指标判别晚更新世以来的海侵地层，对比区域钻孔资料，探讨了泉州湾MIS 3阶段以来的海侵—海退过程。结果表明：Sr/Ba、Mn/Fe在泉州湾不同水深海相沉积物中变化规律明显，适宜作为泉州湾海岸带海相及海陆过渡相沉积物的指相元素，其界限值分别为Sr/Ba>0.16、Mn/Fe<0.23；泉州湾MIS 3阶段以来发生过两次海侵—海退过程。第一次海侵发生于MIS 3阶段，对应区域上的“福州海侵”，其极盛期发生在距今约35 ka；第二次海侵发生在全新世，对应于区域上的“长乐海进”，其极盛期发生在距今约7~4 ka。研究成果对于重建海岸带沉积环境变化历史、深入认识海陆相互作用及预测未来环境变化具有重要意义。
- 泉州湾 /
- 海岸带 /
- MIS 3 /
- 海侵 /
- 地球化学元素比值 /
- 沉积环境
Abstract:
The coastal zone is sensitive to sea–land interaction, making it an ideal place to study the transgression–regression process in Quaternary coastal areas. Based on the stratigraphic and lithologic characteristics of two Quaternary drill cores (DZ01 and DZ02) in the coastal zone of Quanzhou Bay, Fujian Province, a stratigraphic chronological framework was established by using AMS-14C and OSL dating methods. Combined with the statistical analysis results of geochemical element content of indicating facies in modern sediments in Quanzhou Bay, the geochemical element ratios, foraminifers, and ostracods' environmental indicators were used to identify transgressive strata since the Late Pleistocene. The transgression–regression processes since the MIS 3 in Quanzhou Bay were analyzed by comparing it with the regional borehole data. The results show that the Sr/Ba and Mn/Fe values vary significantly in the marine sediments at different water depths in Quanzhou Bay, making them suitable as indicator elements in the marine and sea–land transitional sediments in the Quanzhou Bay coast, with the limit values of Sr/Ba<0.16 and Mn/Fe<0.23, respectively; there have been two transgression–regression processes since the MIS 3 in Quanzhou Bay. The first transgression occurred in the MIS3, corresponding to the regional "Fuzhou transgression," which peaked at about 35 ka B.P. The second transgression occurred in the Holocene, corresponding to the regional "Changle transgression," which peaked at about 7–4 ka B.P. The research results are significant for reconstructing the history of sedimentary environment changes in coastal zones, understanding sea–land interaction, and predicting future environmental changes.
- Quanzhou Bay /
- coastal zone /
- MIS 3 /
- transgression /
- geochemical element ratio /
- sedimentary environment

HTML全文

图 1 研究区及钻孔、取样位置示意图

Figure 1.

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图 2 钻孔年代地层对比

Figure 2.

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图 3 泉州湾海岸带钻孔海侵地层识别和对比

Figure 3.

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图 4 泉州湾沿岸钻孔海侵层对比（剖面位置见图1）

Figure 4.

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图 5 晋江沿岸钻孔海侵层对比（剖面位置见图1）

Figure 5.

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表 1 泉州湾钻孔及样品统计

Table 1. Statistics of the drill cores and samples from Quanzhou Bay

钻孔编号	地理位置	高程/ m	孔深/ m	取芯率/ %	AMS-¹⁴C 样品个数	OSL样品个数	化学元素分析样品个数	微体样品组数
DZ01	晋江河口西岸（118°37′20.68″E，24°51′27.48″N）	28.0	24.1	86.5	5	2	107	9
DZ02	晋江市江头村（118°36′46.84″E， 24°48′27.24″N）	19.0	28.0	92.1	6	1	136	43

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表 2 钻孔AMS-¹⁴C测年结果

Table 2. AMS-¹⁴C test results of the samples from the two drill cores

序号	样品编号	深度/m	样品物质	测试年龄/a BP	校正年龄/Cal a BP
1	DZ01-15	2.65	淤泥	770±20	696±15
2	DZ01-66	9.05	淤泥	6250±25	7196±44
3	DZ01-74	9.85	淤泥	6575±25	7473±30
4	DZ01-¹⁴C-2	11.65	炭屑	11540±100	13373±98
5	DZ01-109	15.85	淤泥	31660±410	35580±430
6	DZ02-15	3.45	淤泥	2615±20	2749±6
7	DZ02-¹⁴C-2	4.95	贝壳碎片	3905±35	4338±56
8	DZ02-¹⁴C-5	12.45	贝壳	6180±50	7081±72
9	DZ02-¹⁴C-7	18.15	炭屑	7620±60	8431±56
10	DZ02-168	21.45	淤泥	8270±35	9264±80
11	DZ02-190	23.65	淤泥	8350±30	9375±49

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表 3 钻孔光释光测年结果

Table 3. OSL test results of the samples from the two drill cores

序号	样品编号	深度/m	U/×10⁻⁶	Th/×10⁻⁶	K/%	等效剂量 /Gy	年剂量/ （Gy/ka）	含水量/%	测试年龄/ka
1	DZ01-OSL-4	19.25	5.09±0.11	14.82±0.38	2.91±0.02	344.90±12.37	5.10±0.31	20±5	67.6±4.7
2	DZ01-OSL-5	20.20	3.42±0.11	17.09±0.44	2.68±0.03	401.85±11.78	4.73±0.28	17±5	85.0±5.6
3	DZ02-OSL-1	24.80	5.83±0.42	19.88±1.20	4.54±0.17	204.36±9.47	6.92±0.40	22±5	29.5±2.2

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表 4 泉州湾海相及过渡相沉积物指相地球化学元素统计特征

Table 4. Statistical characteristics of geochemical elements of indicating facies in the marine and transitional sediments of Quanzhou Bay

沉积物类型	统计类型	Sr/×10^-6	Ba/×10^-6	Sr/Ba	Rb/×10^-6	K/%	Rb/K	Mn/×10^-6	Fe/%	Mn/Fe	有孔虫丰度 /（枚/20 g）	介形类丰度 /（枚/20 g）
泉州湾现代沉积物	平均值	118.68	472.48	0.25	142.70	2.90	0.05	1112.87	5.24	0.23	131.00	96.00
	最大值	199.55	762.10	0.37	175.68	4.35	0.06	1850.53	7.98	0.67	224.00	120.00
	最小值	76.41	305.37	0.17	95.75	2.03	0.04	768.89	2.03	0.15	36.00	80.00
	标准差	22.91	84.81	0.04	13.08	0.44	0.01	254.51	1.34	0.12	84.75	17.28
	变异系数	0.19	0.18	0.17	0.09	0.15	0.10	0.23	0.26	0.51	0.65	0.18
钻孔河口湾相	平均值	88.88	450.03	0.20	142.65	2.58	0.06	1215.79	5.07	0.22	22.86	9.00
	最大值	108.33	497.20	0.24	152.04	2.92	0.06	4060.88	6.88	0.59	86.00	26.00
	最小值	74.80	426.52	0.16	137.20	2.37	0.05	623.39	4.38	0.12	1.00	0.00
	标准差	12.43	23.84	0.03	5.74	0.19	0.002	1256.63	0.85	0.17	36.77	10.02
	变异系数	0.14	0.05	0.15	0.04	0.07	0.04	1.03	0.17	0.76	1.61	1.11
钻孔浅海相	平均值	140.12	438.99	0.32	141.27	2.66	0.05	736.73	4.91	0.15	2612.67	855.67
	最大值	267.82	480.10	0.65	158.18	2.92	0.06	1209.30	5.99	0.23	9536.00	4060.00
	最小值	87.90	400.82	0.19	131.26	2.48	0.05	512.66	4.46	0.11	232.00	34.00
	标准差	63.36	25.18	0.16	8.14	0.12	0.00	241.64	0.45	0.04	3240.64	1170.28
	变异系数	0.45	0.06	0.49	0.06	0.05	0.05	0.33	0.09	0.26	1.24	1.37

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表 5 泉州湾沿岸、晋江沿岸钻孔信息表

Table 5. Drill cores along Quanzhou Bay and Jinjiang Rivers

序号	钻孔编号	钻孔位置	钻孔深度/m	测试数据	资料来源
1	DZ01	晋江河口西岸	24.1	¹⁴C、光释光、粒度、微体等	文中
2	DZ02	晋江市江头村	28.0	¹⁴C、光释光、粒度、微体等	文中
3	CZ01	晋江市杏田村	7.7	¹⁴C、光释光	赵红梅等，2022b
4	ZK301	泉州北门养殖场附近	22.07	微体、孢粉、¹⁴C	程乾盛，1991
5	ZK308	泉州平原入海口附近的池店东侧	24.73	微体、孢粉、¹⁴C	程乾盛，1991
6	QK3-5	浮桥镇新步村	35.69	¹⁴C、光释光	张璞等，2005
7	QZDSZK01	大淮新村刺桐南路	35.1	¹⁴C、光释光	陈大桂等，2016
8	QZDSZK02	池店镇江滨中学	21.6	¹⁴C、光释光
9	QZDSZK03	台商投资区百崎乡煤场南税务局对面砂场	28.7	¹⁴C、光释光
10	QZDSZK04	晋江大桥西南	25.9	¹⁴C、光释光
11	QZDSZK05	延陵村西南	27.7	¹⁴C、光释光

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福建泉州湾海岸带MIS 3阶段以来的海侵—海退过程

1. 中国地质科学院水文地质环境地质研究所，河北 石家庄 050061 2. 中国地质科学院第四纪年代学与水文环境演变重点实验室，河北 石家庄 050061 3. 福建省水循环与生态地质过程重点实验室，福建 厦门 361009

作者简介: 赵红梅（1981—），女，博士，高级工程师，主要从事第四纪地层与沉积环境研究。E-mail：zhmay81@126.com

通讯作者: 毛欣（1989—），男，博士，副研究员，主要从事第四纪环境演变研究。E-mail：maoxin.iheg@cnu.edu.cn

Transgression–regression processes since the MIS 3 in the coastal zone of Quanzhou Bay, Fujian

Corresponding author: MAO Xin, maoxin.iheg@cnu.edu.cn

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中国地质科学院水文地质环境地质研究所，河北石家庄 050061

2.
中国地质科学院第四纪年代学与水文环境演变重点实验室，河北石家庄 050061

3.
福建省水循环与生态地质过程重点实验室，福建厦门 361009